Official Series Description


Lab Data Summary

Aggregate lab data for the NICKEL soil series. This aggregation is based on all pedons with a current taxon name of NICKEL, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to NICKEL were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
4240A0756S1959NM013013Nickel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.2695808,-106.6766815

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NICKEL soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the NICKEL series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the NICKEL series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the NICKEL series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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Competing Series

Soil series competing with NICKEL share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the NICKEL series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the NICKEL series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

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Soil series sharing subgroup-level classification with NICKEL, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. NM-2012-02-14-05 | Hidalgo County - December 1973

    Diagram showing relationship of several soil associations and the topography in Hidalgo County (Soil Survey of Hidalgo County, New Mexico; December 1973).

Map Units

Map units containing NICKEL as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Nipton-Rock outcrop-Nickel family complex, 10 to 50 percent slopes5715461523901rj0az62319941:24000
Nickel-Topawa-Eba families complex, 10 to 50 percent slopes843317515079471mm4gaz62720051:24000
Tumarion-Nickel family complex, 8 to 35 percent slopes1366015079991mm64az62720051:24000
Greyeagle-Continental-Nickel association, 1 to 40 percent slopes6534180531151s8daz64519821:24000
Eba-Nickel-Cave association, 3 to 25 percent slopes397880530681s6waz64519821:24000
Nickel-Cave complex, 8 to 30 percent slopes936340531751sbbaz64519821:24000
Nickel-Cave complex, low precipitation, 8 to 30 percent slopes944120531821sbkaz64519821:24000
Tres Hermanos-Continental-Nickel complex, 2 to 45 percent slopes4357220544681tp1az66319791:24000
Detrital-Nickel family complex, 1 to 4 percent slopes2966538798373vsrzaz69720051:24000
Nickel family-Bluebird complex, 15 to 45 percent slopes9441877798444vsv8az69720051:24000
Tumarion-Nickel family complex, 8 to 35 percent slopes15030197798491vswsaz69720051:24000
Detrital-Nickel complex, dry, 1 to 6 percent slopes2826449798374vss0az69720051:24000
Arizo-Detrital-Nickel complex, 2 to 6 percent slopes521124798356vsrfaz69720051:24000
Nickel-Skelon family-Detrital complex, 3 to 10 percent slopes9519270798443vsv7az69720051:24000
Tumarion-Nickel family complex, moist, 5 to 40 percent slopes15117356798490vswraz69720051:24000
Nickel-Topawa-Eba families complex, 10 to 50 percent slopes969113982201hxywaz69720051:24000
Nickel family extremely gravelly sandy loam, 2 to 35 percent slopes288550544921tptaz69919931:24000
Vace-Nickel complex, 4 to 30 percent slope705396929672762ww2vca79520231:24000
Filaree-Lanip-Nickel association1901023394056hqvqca79520231:24000
Nickel gravelly sandy loam, 3 to 9 percent slopesNC128508570401xc0nm02319671:31680
Lehmans-Nickel association, 1 to 9 percent slopesLN42694570301xbpnm02319671:31680
Eba-Nickel complex, 10 to 60 percent slopesEN31403570031x9tnm02319671:31680
Nickel-Turney association, 0 to 5 percent slopesNT7853570411xc1nm02319671:31680
Nickel gravelly loam, 1 to 5 percent slopesNg2964570421xc2nm02319671:31680
Nickel very gravelly sandy loam, 3 to 9 percent slopesNK68243560561wb8nm02919671:24000
Nickel-Tres Hermanos complexNT42052560571wb9nm02919671:24000
Nickel-Latene associationNL905556701vxtnm60019731:24000
Nickel-Latene associatin, rollingNL11050558181w2lnm61219701:24000
Nickel-Tencee association, strongly slopingNTD38680635678pbgrnm64619761:24000
Nickel-Aztec gravelly sandy loams, 2 to 8 percent slopesNaC4939635677pbgqnm64619761:24000
Nickel very gravelly fine sandy loam, very steep62227215565461wv2nm66019811:48000
Nickel-Chamberino association, gently sloping6376032565471wv3nm66019811:48000
Nickel-Tencee-Delnorte complex, moderately sloping6448904565481wv4nm66019811:48000
Badland-Nickel complex, extremely steep1618583564911ws9nm66019811:48000
Nickel-Upton association, 2 to 15 percent slopes MLRA 423858321593062spssnm66219791:48000
Continental-Nickel association, 0 to 15 percent slopes1010003592762spspnm66219791:48000
Nickel-Caliza very gravelly sandy loams, 1 to 30 percent slopes649202540571621xgynm66419841:24000
Nickel variant very gravelly sandy loam, 2 to 15 percent slopes6382616571571xgsnm66419841:24000
Nickel-Upton associationNU78539634578p9b8nm6901:24000
Nickel-Badland complexNB49554634577p9b7nm6901:24000
Masonfort-Nickel associationMN48893634573p9b3nm6901:24000
Nickel-Bitter Spring associationNIC2469189751721pj7nv60819671:24000
Crosgrain-Irongold-Nickel association24021447468844hqw0nv75520061:24000
Filaree-Lanip-Nickel association19016709468835hqvqnv75520061:24000
Nickel-Arizo association2109088468839hqvvnv75520061:24000
Bard-Nickel-Limewash association2707745468849hqw5nv75520061:24000
Crosgrain-Typic Torriorthents-Nickel association2414853468845hqw1nv75520061:24000
Nickel-Crosgrain association2112961468840hqvwnv75520061:24000
Heleweiser-Upperline-Nickel association2891276469037hr27nv75520061:24000
Canoto-Nickel association20581243469079hr3lnv78519951:24000
Weiser-Nickel association2021834469068hr37nv78519951:24000
Nickel very gravelly fine sandy loam, bedrock substratum, 2 to 8 percent slopes440899469316hrc7nv78819821:24000
Aztec-Nickel-Knob Hill complex, 2 to 15 percent slopes418895469313hrc4nv78819821:24000
Nickel-Crosgrain association21143216809921tf6knv78819821:24000
Nickel-Chispa association, undulatingNcC26614584811yvhtx24319711:31680
Chispa-Nickel association, undulatingCnC13683584661yv0tx24319711:31680
Vieja-Nickel association, hillyVnE13358584961yvztx24319711:31680
Canutio-Nickel association, rollingClD9897584651ytztx24319711:31680

Map of Series Extent

Approximate geographic distribution of the NICKEL soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .